摘要
秦家园铅锌矿床赋存于长城系陇山群地层中,受北北东向断裂构造控制。矿石工业类型地表均为铅锌氧化矿石,地表向下垂高80m以下多为混合或原生矿石。矿石结构主要为碎裂状结构;团块状构造。矿石矿物主要为闪锌矿、方铅矿及其氧化物。具典型的中低温热液充填-交代型矿床特点。具有深部找矿的潜力。
The Qinjiayuan lead-zinc deposit occurs in the Longshan Group strata of the Great Wall System and is controlled by NE-trending faults. The surface of the ore industry type is lead-zinc oxide ore, and most of the ore below 80 m vertical is mixed or primary ore. The ore structure is mainly fractured structure and massive structure. The ore minerals are sphalerite,galena and their oxides. The deposit has typical characteristics of medium-low temperature hydrothermal filling-metasomatic type. It has deep prospecting potential.
引文
[1](《1:25万天水幅区调报告》长安大学李永军等,2003年).
[2](《甘肃省张家川县秦家园铅锌矿普查报告》刘伟等,2008年).
[3](《甘肃省秦家园铅锌矿成矿地质特征及成矿探讨》甘肃科技黎省平等,2011年).
[4](《甘肃省区域成矿及找矿》张新虎等,2012年).
[5](《甘肃省清水-张家川一带1:5万矿产远景调查成果报告》焦阳等,2015年).